Solution
ID: past-exam-of-the-year-2-of-the-earth-sciences-geology-course-of-the-university-of-oxford/2025/paper-3/5/b/solution
Past exam of the year 2 of the earth sciences (geology) course of the University of Oxford 2025 Paper 3 5 b Solution by
Codex 0 2026-10-25
Healthy green vegetation has strong visible absorption in the blue, around –, and red, around –, mainly from chlorophylls and other photosynthetic pigments. Weaker absorption around green wavelengths produces a relative reflectance maximum near and the familiar green appearance. The red edge is the steep reflectance rise around –. In the near-infrared, weak pigment absorption and multiple scattering at internal leaf tissue–air interfaces produce high reflectance, commonly a broad plateau. This plateau is primarily a structural scattering effect, rather than chlorophyll reflecting the light.[ref]
Measuring vegetation by NASA Earth Observatory. “Normalized Difference Vegetation Index”: contrast between chlorophyll absorption of visible light and strong near-infrared scattering by leaf structure.
Qualitative reflectance spectrum of healthy green vegetation
. Original synthetic leaf spectrum with a green maximum, red absorption, red edge, near-infrared plateau and shortwave-infrared water absorption troughs. The curve is illustrative rather than measured; shaded bands exemplify red and near-infrared measurements for a vegetation index. Details.Leaf water produces absorption troughs in the shortwave infrared, especially near and , with weaker features near and . Atmospheric water vapor also strongly absorbs near and , so satellite bands usually avoid the centres of those deep troughs. Drying, senescence, pigment loss and changes in canopy structure alter the spectrum; measured canopy reflectance also includes shadows and the soil background.
To highlight vegetation, assign the near-infrared band to the red display channel, red to green and green to blue: vigorously vegetated areas appear bright red in this conventional false-colour composite. Alternatively calculate the normalized difference vegetation index from atmospherically corrected, spatially registered red and near-infrared reflectances:Large positive values indicate a strong vegetation-like red/NIR contrast. For example, and give about . Mask clouds, their shadows and invalid low-signal pixels. Bare soil usually has a smaller contrast, while water often has negative values; fixed universal thresholds are inappropriate, and dense vegetation can saturate the index. A band ratio improves contrast but is not a direct count of plants or a unique measure of physiological health.[ref]
Measuring vegetation by NASA Earth Observatory. “Normalized Difference Vegetation Index”: normalized red/near-infrared contrast and interpretation of green vegetation.
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